Thursday, 26 March 2015

CHANNEL PROCESSES - Erosion theory

  • Three main processes= erosion, transportation and deposition. 
  • The dominant process operating = depends on the amount of energy available. 
  • Governed - velocity of the flow + the amount of water flowing within the channel (discharge).

Erosion theory.

Rivers erode because they process energy.
Their total energy depends on:
  • weight of the water = the greater the mass of water= more energy it will possess - the influence of gravity on its movement
  •  height of the river above its base level (usually sea level) = source of potential energy + the higher the source of the river =more energy
  • steepness of the channel =  controls the speed of the river= determines how much kinetic energy it has

Kinetic energy
Lost through :
  • through friction
  •  internally through turbulence within the flow of the river, 
  • externally through contact with the bed and banks of the river channel. 
Energy loss through friction = impacts- all parts of a river.

 Upland river channel. 
Channel = rocky bed + many large boulders. 
Rough shape = means that the wetted perimeter (the overall length of the bed and banks that the river is in contact with) = large. 
Energy = lost through friction + the river’s velocity = energy level is reduced. 
Normal conditions= unable to perform much erosion. 
River contains large quantities of water following heavy rain or snowmelt=  energy to perform great amounts of erosion.